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Temperature reconstruction for Arctic glaciers

机译:北极冰川的温度重建

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Numerous data indicate discernible warming of the Northern Hemisphere in the 20th century especially at high latitudes. Summer melting at the surface of Arctic glaciers is likely to increase this warming. To verify this phenomenon, we reconstruct the past temperatures of the Arctic ice caps at their surface and at the 10 m depth. The reconstructions are made for two Arctic ice caps (Austfonna and Akadermii Nauk) by means of the inversion of the measured temperature-depth profiles. In addition, we use the measured oxygen-isotope ratio and the melt feature index as input data. We find that the present ice temperature is the highest over the last 1000 years, while the lowest temperature occurred in the 1700s. The surface temperature variations of Akadermi Nauk (Severnaya Zemlya) and Austfonna (Svalbard) Ice Caps exceed the average Arctic temperature anomalies over the last 150 years by 6 to 7 degrees C. (c) 2006 Elsevier B.V. All rights reserved.
机译:大量数据表明,在20世纪特别是在高纬度地区,北半球变暖。夏季,北极冰川表面的融化可能会加剧这种变暖。为了验证这一现象,我们重建了北极冰盖表面和深度10 m的过去温度。通过对测得的温度-深度剖面进行反演,对两个北极冰盖(Austfonna和Akadermii Nauk)进行了重建。另外,我们使用测得的氧同位素比和熔体特征指数作为输入数据。我们发现,目前的冰温在过去1000年中最高,而最低温度发生在1700年代。 Akadermi Nauk(Severnaya Zemlya)和Austfonna(Svalbard)冰帽的表面温度变化在过去150年中超过了北极平均温度异常6-7摄氏度。(c)2006 Elsevier B.V.保留所有权利。

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